Basic features of the vertical structure of a sand-wind flow over the surface of spits and bars of the Black and Azov Seas coastal zone were studied within 17 main sites. The middle diameter, sorting coefficient, and leading fraction of the drift vertical distribution were represented during coastal natural experiments. Wind velocities were from 5 to 26 m/s. Aeolian differentiation stipulates changes of beach sediments from coarse to fine sands in various aeolian relief forms. These forms contain two basic fractions of the sediments (80 - 95 %) - 0,1 - 0,25 mm and 0,25 - 0,5 mm in different sandy sea-shores.

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